成都理工大学学报(自然科学版)
成都理工大學學報(自然科學版)
성도리공대학학보(자연과학판)
Journal of Chengdu University of Technology (Science & Technology Edition)
2015年
5期
530-538
,共9页
王鹏万%张磊%邹辰%宋海强%陈子炓%王高成%李君军%李庆飞
王鵬萬%張磊%鄒辰%宋海彊%陳子炓%王高成%李君軍%李慶飛
왕붕만%장뢰%추신%송해강%진자료%왕고성%리군군%리경비
镇雄-赫章地区%高演化%筇竹寺组%页岩气%勘探方向
鎮雄-赫章地區%高縯化%笻竹寺組%頁巖氣%勘探方嚮
진웅-혁장지구%고연화%공죽사조%혈암기%감탐방향
Zhenxiong-Hezhang area%high maturity%Qiongzhusi Formation%shale gas%exploration direction
勘探实践表明中国西南的镇雄-赫章地区下寒武统筇竹寺组页岩气成藏条件优越,受强改造与高演化制约,筇竹寺组页岩气勘探尚未获得突破。为寻找热演化程度相对较低的有利保存区,基于钻井、露头、地震资料,通过编制关键期次岩相古地理图及古地质图,结合各沉积-剥蚀分区典型埋藏史分析,精细刻画镇雄-赫章地区沉积-剥蚀分区特征。结果表明:镇雄-赫章地区发育加里东期-海西期古隆起,控制二叠纪前沉积充填过程,沉积-剥蚀差异性明显。其中Ⅰ区及Ⅱ区缺失层系较多,且热演化间断时间长,热演化程度相对较低,为筇竹寺组页岩气有利勘探区。古隆起及周缘地区为海相高演化页岩气勘探的有利指向。
勘探實踐錶明中國西南的鎮雄-赫章地區下寒武統笻竹寺組頁巖氣成藏條件優越,受彊改造與高縯化製約,笻竹寺組頁巖氣勘探尚未穫得突破。為尋找熱縯化程度相對較低的有利保存區,基于鑽井、露頭、地震資料,通過編製關鍵期次巖相古地理圖及古地質圖,結閤各沉積-剝蝕分區典型埋藏史分析,精細刻畫鎮雄-赫章地區沉積-剝蝕分區特徵。結果錶明:鎮雄-赫章地區髮育加裏東期-海西期古隆起,控製二疊紀前沉積充填過程,沉積-剝蝕差異性明顯。其中Ⅰ區及Ⅱ區缺失層繫較多,且熱縯化間斷時間長,熱縯化程度相對較低,為笻竹寺組頁巖氣有利勘探區。古隆起及週緣地區為海相高縯化頁巖氣勘探的有利指嚮。
감탐실천표명중국서남적진웅-혁장지구하한무통공죽사조혈암기성장조건우월,수강개조여고연화제약,공죽사조혈암기감탐상미획득돌파。위심조열연화정도상대교저적유리보존구,기우찬정、로두、지진자료,통과편제관건기차암상고지리도급고지질도,결합각침적-박식분구전형매장사분석,정세각화진웅-혁장지구침적-박식분구특정。결과표명:진웅-혁장지구발육가리동기-해서기고륭기,공제이첩기전침적충전과정,침적-박식차이성명현。기중Ⅰ구급Ⅱ구결실층계교다,차열연화간단시간장,열연화정도상대교저,위공죽사조혈암기유리감탐구。고륭기급주연지구위해상고연화혈암기감탐적유리지향。
The exploration practice shows that the shale gas accumulation condition of the Lower Cambrian Qiongzhusi Formation in the Zhenxiong-Hezhang area is superior.Being limited in the strong transformation and high maturity,the shale gas exploration in Qiongzhusi Formation has not been won a breakthrough.In order to search out the favorable preservation areas with relatively low thermal evolution degree,based on the drilling,outcrop and seismic data,through plotting the lithofacies-paleogeographic map and ancient geological map of the key periods,and combined with the analysis of the typical buried history of every deposition-denudation division,this paper describes the characteristics of the sedimentary-denudation divisions in the Zhenxiong-Hezhang area.The results show that there develops the Caledonian-Hercynian ancient uplift in this area,which controls the sedimentary process before Permian and that the deposition-denudation difference is obvious.In District Ⅰ and District Ⅱ,there is lack of more strata,the thermal evolution intermittent time is long,and the Permian thermal evolution degree is relatively low,so District Ⅰ and District Ⅱ are the favorable exploration areas of the shale gas in Qiongzhusi Formation.The ancient uplift and peripheral regions are the favorable targets for the explorating the highly mature shale gas.